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doi: 10.1152/jn.00154.2010, 21
Peroxisome biogenesis and function: September 11, 2009

It is logical then, that the final Si/Al ratio in a zeolite determines the ion exchange capacity and attraction of cations that come to reside inside the pores and channels (Mumpton, 1999

Similar content being viewed by others Log in or create a free account to read this content Gain free access to this article, as well as selected content from this journal and more on nature.com or References Niforou K, Cheimonidou C, Trougakos IP
